Comparison of Tropospheric Temperature Profiles from Ground-based Microwave Radiometer and Radiosonde at Xi’an, Central China

Kuifeng Zhao, Zipeng Dong, Xingmin Li, Chuang Chen, Yan Peng
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Abstract

The reliability and accuracy of temperature profiles retrieved by ground-based microwave radiometer (MWR) using neural networks at Jinghe meteorological station (Xi’an, China) was evaluated by comparing the temperature retrievals against simultaneous radiosonde observations. For the comparison purposes, temperature measurements from MWR and radiosonde with altitude difference of less than 10 m and time difference of less than 5 minutes were matched with each other. Finally, a total of 1240 pairs of profiles have been compared for the period from June 2017 to July 2019. The MWR-derived temperature showed consistent negative bias of 0.14–2.44 °C throughout the retrieved profile except at 10 km where with a value of +0.22 °C. The root mean square error is less than 2°C for heights below 100 m, and rapidly increases to 4°C at 2 km and remained stable thereafter. Linear regression between temperature derived from MWR and radiosonde at different altitudes indicated that both the slope and intercept showed altitude-dependent behavior. Fairly good agreement between radiosonde and MWR-derived temperature is observed in the lowest 1 km, with linear regress slopes between 0.91–1.00 and correlation coefficients exceeding 0.96. However, both the slope and intercept decreased dramatically with height. The altitude variations of the slope and intercept suggest that the MWR tends to overestimate the temperature in cold season but underestimate the temperature in warm season in the middle and upper troposphere. Temperature gradient derived from radiosonde showed that the occurrence frequency of temperature inversions peaked at 28% at near surface at Xi’an, and declined to 8% at 2 km. MWR failed to distinguish the temperature inversion in most cases. The missed detection ratio is approximately 40% at surface and beyond 80% at altitude higher than 500 m. There is still big room for improving the accuracy of the temperature retrievals of MWR, especially in the aspect of temperature inversion detection. Our findings suggest that the MWR data needs to be used with caution in the air pollution study.
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西安地面微波辐射计和探空仪对流层温度廓线的比较
通过与探空同时观测数据的对比,评价了基于神经网络的地面微波辐射计在西安泾河气象站反演温度廓线的可靠性和准确性。为了进行对比,我们将高度差小于10 m、时差小于5 min的MWR和探空测温数据进行匹配。最后,对2017年6月至2019年7月期间的1240对剖面进行了比较。在整个反演剖面中,mwr衍生的温度显示出一致的负偏差,为0.14-2.44°C,但在10 km处的值为+0.22°C。在海拔100 m以下,均方根误差小于2°C,在海拔2 km处,均方根误差迅速增大到4°C,此后保持稳定。在不同海拔高度,MWR和探空温度的线性回归表明,坡度和截距都表现出高度依赖性。在最低1 km范围内,探空温度与水波源温度的线性回归斜率在0.91 ~ 1.00之间,相关系数超过0.96。然而,随着高度的增加,斜率和截距都急剧减小。坡度和截距的高度变化表明,MWR在冷季有高估对流层中高层温度的趋势,而在暖季有低估对流层中高层温度的趋势。探空温度梯度结果表明,西安近地表逆温发生频率最高,为28%,2 km处降至8%。在大多数情况下,MWR不能区分逆温。地表漏检率约为40%,海拔500米以上的漏检率超过80%。MWR的温度反演精度还有很大的提升空间,特别是在温度反演检测方面。我们的研究结果表明,在空气污染研究中需要谨慎使用MWR数据。
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